The system at
toward the quasar J2233-606
has saturated hydrogen lines (from Ly-
up to Ly-8)
and metal lines of
C II, Si II, Si III,
C IV, and Si IV.
The results obtained with the MCI
are presented in Table 1 and illustrated in
Figs. 1 and 2.
Parts of profiles included in the
minimization
are marked by horizontal lines at the panel bottoms in Fig. 1.
Profiles of the doublet N V
Å and
N V
Å were
calculated later using the obtained velocity and density
distribution and the metallicity derived from the fitting of
N III
Å.
It is seen from Fig. 1 that most spectral features can be well
represented assuming uniform
metallicities and a common HM UV background.
Figure 2 demonstrates the distribution of the
radial velocity and gas density (panels a and b)
along the line
of sight (rearranged in accord with the principle
of minimal entropy production rate).
The density distributions for the ions involved in the optimization
are shown in panels c-j,
whereas the density-weighted velocity distributions which
determine the shapes of the spectral lines are presented in
Fig. 3.
This figure shows that the density-weighted
velocity distributions
for low ions C II and Si II are similar, but
differ from those for high ions C IV and Si IV.
These distributions easily explain why the lines of C II and
Si II look very much alike and why their centers are displaced
by
km s-1 (DP)
with respect to C IV and Si IV.
The study of this system by DP,
who used the standard Voigt profile fitting,
produced comparable column densities (albeit 20-50% smaller).
However, the metallicities obtained by DP for two main clouds
(at v = 0 km s-1 and v = -43 km s-1) differ
nearly by two orders
of magnitude: [X/H] = -0.9 and -2.7, respectively
(in our case [X/H]
for the whole system).
As shown in Paper I,
the Voigt fitting may in general yield correct column densities
when applied to unsaturated lines, but the mean U and, hence,
the ionization corrections may not be unambiguous.
Therefore,
the conclusion made by DP that the
system contains
"a region of intense star-formation activity'' may not be well justified
since this result is model dependent.
The values of the average gas density n0 and kinetic temperature
,
and the
cloud thickness Lestimated in our model (see Table 1)
are typical for the Ly-
systems discussed in the literature
(e.g., Giallongo & Petitjean 1994; Viegas et al. 1999;
Prochaska & Burles 1999; Chen et al. 1998; Chen et al. 2001).
Low metallicity for the whole system ([X/H] < -2.0)
and its dimension of 20 kpc imply that this system can originate
in a galactic halo or in a large scale structure object.
This system exhibits a plenty of metal lines in different ionization stages.
The metal profiles are not very complex
and extend over the velocity range from -100 km s-1
to 100 km s-1.
Results obtained with the MCI are presented in Table 1 and
shown in Figs. 4 and 5. As in the previous system, most absorption
features can be well
described with uniform metallicities and a common HM spectrum.
The Ly-
profile is contaminated by the forest absorption
in the blue and red wings and therefore the Ly-
absorption feature
was not involved in the analysis.
The profiles of Mg II
Å
and Al II
Å were computed later using the
derived velocity and density distributions.
Mg II
Å
is contaminated by a telluric line and this explains
the difference between the computed and observed profiles.
The synthetic and observed profiles of Al II
Å
show much more pronounced discrepancy.
Fractional ionisation curves for Al II and Al III
were computed with CLOUDY.
These curves allowed us to fit the Al III doublet quite well
with the Al abundance similar to that obtained for the other metals.
However, when
the Al II profile was included
in the fitting, the Al metallicity differed by order
of magnitude from the other metals. Besides
it was impossible to fit adequately the Al III doublet.
Similar behaviour of Al was reported also by DP who noted
that "the recombination coefficients used to compute the
aluminium ionisation equilibrium
[in CLOUDY] are probably questionable''.
Column densities derived by DP coincide well (within 15%) with
that obtained in our procedure except for the
saturated Si III
Å line for which the Voigt
fitting gave nearly 2 times lower value.
The abundances estimated in DP scatter again from component
to component, but nevertheless they conclude that
"the gas in this system
is likely of quite high metallicity (larger than 0.1 solar)''.
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Figure 6:
Same as Fig. 1 but for the
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Similar to the Voigt fitting,
the MCI also delivered for this system high metal abundancies:
one third solar for carbon and silicon and nearly
two times lower for nitrogen, magnesium and aluminium.
Taking into account this result and a compact dimension
(5 kpc, see Table 1)
of the absorbing region we come to the same conclusion as
Prochaska & Burles (1999) did: the system at z = 1.94 can hardly
be a large scale structure object (like a filament or a wall)
and should be related to a galactic system (may be a region of intense star
formation).
This is the most interesting system from the family of the absorbers at z = 1.9 toward J2233-606. The metal line profiles show a rather complex structure extending over the velocity range of about 700 km s-1. Some of these profiles are severely blended that hampers the unique Voigt profile deconvolution (e.g. DP assumed 17 components to describe metal profiles).
The MCI code turned out to be much more robust
and was able to recover the self-consistent line profiles even under such
unfavourable conditions. The physical parameters which the MCI delivered
for the z = 1.87 system together with
the underlying velocity and density distributions
are presented in Table 1 and in Figs. 6 and 7. It is seen from Fig. 6
that like in the previous two systems all lines are well described
with a single parameter set, uniform metallicities and a common
HM UV background.
The blue wing of the Ly-
line is contaminated by the forest
absorption as is clearly seen from the Ly-
and Ly-
profiles.
The synthetic
profile of the O VI
Å line
was calculated later using the derived best fitting
parameters and the oxygen abundance [O/H] = -1.0(which is about 3 times over the other
element abundances from this system).
Even with the increased abundance
the synthetic profile of O VI is still much weaker than the observed
intensities. This discrepancy
rules out the ionization of O VI by the adopted background
radiation.
Taking into account that all other elements have been well
described with a given HM spectrum and that the collisional ionization
of oxygen
can hardly be effective at low densities (
)
and temperatures of
K,
this result seems to favor the interpretation that
the O VI ion and the other ions do not arise
in the same gas (Kirkman & Tytler 1999; Reimers et al. 2001).
According to our results, the absorber at z = 1.87 could be a large size cloud with very high velocity dispersion. Its estimated linear size of 80 kpc is consistent with dimensions of extended gaseous envelopes observed around galaxies at z < 1. In these envelopes, Mg II absorption is the dominant observational signature at the distancies up to a few tens of kiloparsecs (Bergeron & Boissé 1991), whereas highly ionizied species like C IV are observed at distances of at least 100 kpc from galactic centers (Chen et al. 2001). Since the extended structure of the same order of magnitude is observed at z = 1.87, we may conclude that this system arises in the external halo at large galactocentric distances.
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Figure 7:
Same as Fig. 5 but for the
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Copyright ESO 2002